Geology of Japan

The geological features and bedrock composition of Japanese Islands
The island of Japan was separated from mainland Asia by back-arc spreading

Formation of Japanese Islands

The islands of Japan are primarily the result of several large ocean movements occurring over hundreds of millions of years from the mid-Silurian to the Pleistocene as a result of the subduction of the Philippine Sea Plate beneath the continental Amurian Plate and Okinawa Plate to the south, and subduction of the Pacific Plate under the Okhotsk Plate to the north.

Around 23 million years ago, the now Western Japan was a coastal region of the Eurasia continent. The subducting plates, being deeper than the Eurasian plate, pulled parts of Japan which become modern Chūgoku region and Kyushu eastward, opening the Sea of Japan (simultaneously with the Sea of Okhotsk) around 15-20 million years ago, with likely freshwater lake state before the sea has rushed in.[1] Around 16 million years ago, in Miocene period, a peninsula attached to the eastern coast of the Eurasian continent was well formed. About 11 million years before present, the parts of Japan which become modern Tohoku and Hokkaido were gradually uplifted from the seafloor, and terranes of Chūbu region were gradually accreted from the colliding island chains. The Strait of Tartary and the Korea Strait opened much later, about 2 million years ago. At the same time, a severe subduction of Fossa Magna graben have formed the Kantō Plain.[2]

Geological composition

General information

Overall, the geological composition of Japan is poorly understood. Japanese islands are formed of several geological units parallel to the subduction front. The parts of islands facing oceanic plates are typically younger and display larger proportion of volcanic products, while the parts facing Sea of Japan are mostly heavily faulted and folded sedimentary deposits. In north-west Japan, the thick quaternary deposits make determination of the geological history especially difficult.[3]

Geological structure

The Japanese islands are divided into three major geological domains:

Research on Geology of Japan

The Geology of Japan is handled mostly by Geological Society of Japan (日本地質学会), with following major periodicals:

Current geological hazards of Japanese Islands

Japan is situated in a volcanic zone on the Pacific Ring of Fire. Frequent low intensity earth tremors and occasional volcanic activity are felt throughout the islands. Destructive earthquakes, often resulting in tsunamis, occur several times a century. The most recent major quakes include the 2011 Tōhoku earthquake and tsunami, the 2004 Chūetsu earthquake and the Great Hanshin earthquake of 1995. Hot springs are numerous and have been developed as resorts.

See also

References

Further reading

  • Hashimoto, M., ed. (1990). Geology of Japan. Dordrecht: Kluwer Academic Publishers. ISBN 9780792309093. 
  • T. Moreno (Editor), S.R. Wallis (Editor), T. Kojima (Editor), W. Gibbons (Editor) (ed.). Geology of Japan (Geological Society of London)(2015). ISBN 978-1862397439. 

by - (Author),

  • Takai, Fuyuji; Tatsurō Matsumoto; Ryūzō Toriyama (1963). Geology of Japan. University of California Press. 
External image
Statistical map of location, size and depth of earthquakes near Japan


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.